Sand boil

 ( Sand ) 

Sand boils, sand volcanoes, or sand blows occur when water under pressure wells up through a bed of sand. The water looks like it is boiling up from the bed of sand, hence the name.

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Sand volcano A sand volcano or sand blow is a cone of sand formed by the ejection of sand onto a surface from a central point. The sand builds up as a cone with slopes at the sand's angle of repose. A volcanic crater is commonly seen at the summit. The cone looks like a small volcanic cone[1] Images after 2010 Canterbury earthquake and can range in size from millimetres to metres in diameter.

The process is often associated with soil liquefaction and the ejection of fluidized sand that can occur in water-saturated sediments during an earthquake. The New Madrid seismic zone exhibited many such features during the 1811–1812 New Madrid earthquakes. Adjacent sand blows aligned in a row along a linear fracture within fine-grained surface sediments are just as common, and can still be seen in the New Madrid area.

These earthquakes also caused the largest known sand boil in the world, which can still be found near Hayti, Missouri and is locally called "The Beach". It is 2.3 kilometers long and covers 55 hectares.

In the past few years, much effort has gone into the mapping of liquefaction features to study ancient earthquakes. The basic idea is to map zones that are susceptible to the process and then go in for a closer look. The presence or absence of soil liquefaction features, such as , is strong evidence of past earthquake activity, or lack thereof.

These are to be contrasted with , which occur in areas of geyser or subsurface gas venting.

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Flood protection structures Sand boils can be a mechanism contributing to liquefaction and levee failure during . Boil refers to the visible "boiling" movement of coarse sand grains retained in the hole even as finer particles (silts and fine sands) are carried out and deposited on the apron around the boil hole. Sand boils are caused by hydraulic head in levee or dike pushing the water to seep out the other side, most likely during a flood. Sand boils start as simple of laminar flow. With increasing head from rising flood waters, turbulent flow will initiate where the laminar flow leaves the soil to flow freely. Turbulent flow produces soil piping, whereby backward erosion results in a pipe-shaped cavity reaching back into the embankment, initiating at the seep and working through the embankment back to the water source. Once initiated, an unmitigated soil pipe can proceed quickly to embankment failure.

The flow in a sand boil can be slowed, but it is impractical to stop completely. The most effective response to an active sand boil is to stand water over the boil deep enough to reduce the hydraulic gradient and slow the water flow to eliminate turbulence and backward erosion at the head of the pipe. Slower, nonturbulent flow will not be able to move soil particles. The suppressing depth of water is created with forming a stacked ring around the boil. UC Davis, Department of Civil & Environmental Engineering: Photograph of sandbag ring

During the flood of spring 2011, the United States Army Corps of Engineers had to work to contain the largest active sand boil ever discovered. The sand boil measured nine by 12 meters (30 by 40 feet) and was located in the city of Cairo, Illinois, at the confluence of the Mississippi River and the Ohio River. wpsdlocal6.com

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Earthquakes An example of this is during the 1989 Loma Prieta earthquake in San Francisco, when sand boils brought up debris from the 1906 earthquake. This process is a result of liquefaction. By mapping the location of sand boils that erupted in the Marina District during the 1989 Loma Prieta earthquake, scientists discovered the site of a lagoon that existed in 1906. The lagoon developed after the Fair's Seawall was constructed and, in preparation for the Panama–Pacific International Exposition in 1915, was filled in.

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See also

• Internal erosion
• Quicksand
• Seepage

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